Gail L Christeson
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Explore the profile of Gail L Christeson including associated specialties, affiliations and a list of published articles.
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6
Citations
206
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Recent Articles
1.
Cockell C, Schaefer B, Wuchter C, Coolen M, Grice K, Schnieders L, et al.
Front Microbiol
. 2021 Jul;
12:668240.
PMID: 34248877
We report on the effect of the end-Cretaceous impact event on the present-day deep microbial biosphere at the impact site. IODP-ICDP Expedition 364 drilled into the peak ring of the...
2.
Kring D, Tikoo S, Schmieder M, Riller U, Rebolledo-Vieyra M, Simpson S, et al.
Sci Adv
. 2020 Jun;
6(22):eaaz3053.
PMID: 32523986
The ~180-km-diameter Chicxulub peak-ring crater and ~240-km multiring basin, produced by the impact that terminated the Cretaceous, is the largest remaining intact impact basin on Earth. International Ocean Discovery Program...
3.
Gulick S, Bralower T, Ormo J, Hall B, Grice K, Schaefer B, et al.
Proc Natl Acad Sci U S A
. 2019 Sep;
116(39):19342-19351.
PMID: 31501350
Highly expanded Cretaceous-Paleogene (K-Pg) boundary section from the Chicxulub peak ring, recovered by International Ocean Discovery Program (IODP)-International Continental Scientific Drilling Program (ICDP) Expedition 364, provides an unprecedented window into...
4.
Lowery C, Bralower T, Owens J, Rodriguez-Tovar F, Jones H, Smit J, et al.
Nature
. 2018 Jun;
558(7709):288-291.
PMID: 29849143
The Cretaceous/Palaeogene mass extinction eradicated 76% of species on Earth. It was caused by the impact of an asteroid on the Yucatán carbonate platform in the southern Gulf of Mexico...
5.
Schulte P, Alegret L, Arenillas I, Arz J, Barton P, Bown P, et al.
Science
. 2010 Mar;
327(5970):1214-8.
PMID: 20203042
The Cretaceous-Paleogene boundary approximately 65.5 million years ago marks one of the three largest mass extinctions in the past 500 million years. The extinction event coincided with a large asteroid...
6.
Christeson G, McIntosh K, Karson J
Nature
. 2007 Jan;
445(7126):418-21.
PMID: 17251977
At mid-ocean ridges with fast to intermediate spreading rates, the upper section of oceanic crust is composed of lavas overlying a sheeted dyke complex. These units are formed by dykes...